评估热带湿地的甲烷排放:来自全球尺度自然变率和驱动因素的不确定性

IF 5.4 2区 地球科学 Q1 ENVIRONMENTAL SCIENCES Global Biogeochemical Cycles Pub Date : 2023-08-25 DOI:10.1029/2022GB007601
F. Murguia-Flores, V. J. Jaramillo, A. Gallego-Sala
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引用次数: 0

摘要

热带湿地的甲烷排放量占全球湿地排放量的一半,但热带甲烷来源的范围仍存在不确定性。一个限制是将热带湿地视为一个单一的生态系统,特别是在全球陆地表面模型中。我们估计CH4排放量,并评估其环境和人为驱动因素。我们创建了一个包含101项研究的数据集,涉及328点测量,将这些地点分为四种湿地类型,并包括相关的生物和环境信息。我们估计热带湿地的全球CH4排放率为35(5-160)mg CH4 m−2 d−1(中位数、第一和第三个四分位数),全球年排放率为94(56158)Tg y−1。不同湿地类型的通量不同,但除了人为因素外,由于通量变化很大,甚至在湿地类型内,也无法定量确定全球范围内的重要环境驱动因素。沿海湿地产生的中位排放量为12(5-23)Tg y−1。内陆深水湿地排放53(32-114)Tg y−1,面积范围变化很大。内陆浅水湿地的排放量为52(33-78)Tg y−1,随地下水位季节变化而变化。人造湿地排放17(10−4)Tg y−1。农业的污染和氮输入是热带湿地排放的重要人为驱动因素。在估计全球排放量及其对全球变化的具体脆弱性时,需要根据湿地类型考虑变化的具体驱动因素。此外,在实施旨在减少甲烷排放的湿地管理实践时,应考虑这些差异。
本文章由计算机程序翻译,如有差异,请以英文原文为准。

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Assessing Methane Emissions From Tropical Wetlands: Uncertainties From Natural Variability and Drivers at the Global Scale

Methane (CH4) emissions from tropical wetlands represent half of the global wetland emissions, but uncertainties remain concerning the extent of tropical methane sources. One limitation is to conceive tropical wetlands as a single ecosystem, especially in global land surface models. We estimate CH4 emissions and assess their environmental and anthropogenic drivers. We created a data set with 101 studies involving 328-point measurements, classified the sites into four wetland types, and included relevant biological and environmental information. We estimate the global CH4 emission rate from tropical wetlands as 35 (5–160) mg CH4 m−2 d−1 (median, first and third quartile) and an annual global rate of 94 (56, 158) Tg y−1. Fluxes differed among the wetland types, but except for anthropogenic factors, significant environmental drivers at the global scale could not be quantitatively identified because of high flux variability, even within wetland types. Coastal wetlands generate median emissions of 12 (5–23) Tg y−1. Inland deep-water wetlands emit 53 (32–114) Tg y−1, with highly variable areal extent. Emissions from inland shallow-water wetlands are 52 (33–78) Tg y−1 with variation due to seasonal changes in water table level. Human-made wetlands emit 17 (10−4) Tg y−1. Pollution and N inputs from agriculture are significant anthropogenic drivers of emissions from tropical wetlands. Specific drivers of change need to be considered according to wetland type when estimating global emissions as well as their specific vulnerability to global change. Additionally, these differences should be considered when implementing wetland management practices aimed at decreasing methane emissions.

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来源期刊
Global Biogeochemical Cycles
Global Biogeochemical Cycles 环境科学-地球科学综合
CiteScore
8.90
自引率
7.70%
发文量
141
审稿时长
8-16 weeks
期刊介绍: Global Biogeochemical Cycles (GBC) features research on regional to global biogeochemical interactions, as well as more local studies that demonstrate fundamental implications for biogeochemical processing at regional or global scales. Published papers draw on a wide array of methods and knowledge and extend in time from the deep geologic past to recent historical and potential future interactions. This broad scope includes studies that elucidate human activities as interactive components of biogeochemical cycles and physical Earth Systems including climate. Authors are required to make their work accessible to a broad interdisciplinary range of scientists.
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